Documentation

TauCeti.Analysis.Complex.UpperHalfPlane.Geodesic.Segment

Geodesic segments and the convexity of half-planes #

UpperHalfPlane.geodesicSegment z w is the geodesic segment from z to w: the image of [0, dist z w] under the geodesic line geodesicBetween z w. The point-keyed API lives in the UpperHalfPlane namespace (UpperHalfPlane.mem_geodesicSegment_iff, UpperHalfPlane.geodesicSegment_comm, UpperHalfPlane.isCompact_geodesicSegment, …), and segments transform naturally under PSL(2, ℝ) (smul_geodesicSegment).

Along any geodesic line the real part is monotone or antitone (monotone_re_geodesicLine_or_antitone); the set of parameters at which a geodesic line lies in a given half-plane or its closure is an interval (ordConnected_preimage_geodesicLine_rightHalfPlane and companions); and half-planes and their closures are convex: they contain the segment between any two of their points (geodesicSegment_subset_rightHalfPlane, …, geodesicSegment_subset_closure_leftHalfPlane). Convexity is what makes the triangles and polygons bounded by such half-planes convex. An interior point of an interval in a closed half-plane lies in the open half-plane unless the supporting lines coincide (geodesicLine_mem_leftHalfPlane_of_mem_closure).

Source: Walkden, Hyperbolic geometry (MATH32051 lecture notes, Manchester 2019), §7.1 (the segment [z, w]) and Solution 14.1 (half-planes are convex); Katok, Fuchsian groups, geodesic flows…, Clay Math. Proc. 10 (2010), Theorem 3.1 p. 10 (geodesics are semicircles and vertical rays).

Segments #

The geodesic segment from z to w, unfolded: the image of [0, dist z w] under the geodesic line from z to w.

@[simp]

z lies on the segment from z to w.

@[simp]

w lies on the segment from z to w.

@[simp]

The segment from a point to itself is that point.

The segment does not depend on the order of its endpoints.

@[simp]

The segment between two points of a unit-speed geodesic is the image of the interval between their parameters. The parameters may be given in either order.

@[simp]

Segments transform naturally under the action.

The real part is monotone along a geodesic line #

Along a geodesic line the real part is monotone or antitone: the line is a vertical ray or a semicircle centred on the real axis, traversed once. Source: Katok, Fuchsian groups, geodesic flows… (Clay Math. Proc. 10), Theorem 3.1 p. 10.

The parameters at which a geodesic line lies in an open right half-plane form an interval.

The parameters at which a geodesic line lies in the closure of a right half-plane form an interval.

The parameters at which a geodesic line lies in an open left half-plane form an interval.

The parameters at which a geodesic line lies in the closure of a left half-plane form an interval.

An interior point of a geodesic interval in a closed half-plane is strictly in that half-plane unless the two supporting geodesic lines coincide.

Half-planes are convex #

Open right half-planes are convex. Source: Walkden, Hyperbolic geometry (MATH32051), Solution 14.1.